A Preliminary Disease Survey in the Wild Nile Crocodile (Crocodylus Niloticus) Population in the Okavango Delta, Botswana
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Ramsar Information Sheet
Ramsar Information Sheet Text copy-typed from the original document. 1. Date this sheet was completed: 20.11.1996 2. Country: Botswana 3. Name of wetland: The Okavango Delta System 4. Geographical co-ordinates: The Okavango Delta System lies between Longitudes 21 degrees 45 minutes East and 23 degrees 53 minutes East; and Latitudes 18 degrees 15 minutes South and 20 degrees 45 minutes South. It includes the Okavango River, commonly referred to as the Pan handle; the entire Okavango Delta; Lake Ngami; and parts of the Kwando and Linyanti River systems that fall west of the western boundary of the Chobe National Park. The entire area is as depicted on the attached map. 5. Altitude: Generally between 930 metres and 1000 metres above sea level. 6. Area: Approximately 68 640 km² (6 864 000 hectares) 7. Overview Three main features characterise the region, the Okavango, the Kwando and Linyanti river system connected to the Okavango Delta through the Selinda spillway and the intervening and surrounding dryland areas. These features are located within the Okavango rift, a geological structure subject to tectonis control and infilled with Kahalari Group sediments, principally sand, up to 300 metres thick. The Delta is the most important of the above named features. It is an inland delta in a semi arid region in which inflow fluctuations result in large fluctuations in flooded area (10,000 - 16,000 km²), which is comprised of permanent swamp, seasonal swamp and intermittently flooded areas. Similar flooding takes place in the Kwando/Linyanti river system. This leads to high seasonal concentrations of birdlife and wildlife, giving the area a very high tourism potential. -
Final Report: Southern Africa Regional Environmental Program
SOUTHERN AFRICA REGIONAL ENVIRONMENTAL PROGRAM FINAL REPORT DISCLAIMER The authors’ views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States government. FINAL REPORT SOUTHERN AFRICA REGIONAL ENVIRONMENTAL PROGRAM Contract No. 674-C-00-10-00030-00 Cover illustration and all one-page illustrations: Credit: Fernando Hugo Fernandes DISCLAIMER The authors’ views expressed in this publication do not necessarily reflect the views of the United States Agency for International Development or the United States government. CONTENTS Acronyms ................................................................................................................ ii Executive Summary ............................................................................................... 1 Project Context ...................................................................................................... 4 Strategic Approach and Program Management .............................................. 10 Strategic Thrust of the Program ...............................................................................................10 Project Implementation and Key Partners .............................................................................12 Major Program Elements: SAREP Highlights and Achievements .................. 14 Summary of Key Technical Results and Achievements .......................................................14 Improving the Cooperative Management of the River -
Continental Slope Communities Tom Laidig
Continental Slope Communities Tom Laidig Summary and Introduction In the shallow coastal areas of the Gulf of the Farallones, as in other regions of the world, fishing pressure has increased and numbers of fish have decreased over the past few decades. As many fish stocks have declined, some fishermen have been forced to look elsewhere to fill their nets. Traditional fishing grounds in the gulf have been located on the Continental Shelf, a rather flat, relatively shallow area of the sea floor adjacent to the coast. At a depth of about 200 m (660 ft), the bottom starts to drop off more rapidly on what is called the Continental Slope. It is on upper and middle parts of this steeper slope that the new fishing grounds have been established. Because the fish inhabiting these deeper waters are less understood than those in shallower water, there is a danger of overharvesting, which could threaten the long- term viability of these newer fisheries. The deep waters of the Continental Slope are characterized by nearly freezing temperatures, extremely low light conditions, and very high pressures. Because of the cold, organisms that live at these depths have slower metabolisms—they eat less frequently, are slower in digesting their food, and move and grow more slowly. They also attain greater ages than their counterparts that live in shallower waters—some deep-sea rockfish live more than 70 years. Many of the animals living in the perpetual darkness of the Continental Slope have developed light-producing organs. These serve various functions, such as communicating with members of their own kind (as in courtship), attracting food (like attracting moths to a flame), and avoiding being eaten (flashing a light in a predator’s eyes can give an animal a chance to get away). -
The Hydrology of the Okavango Delta, Botswana—Processes, Data and Modelling
Regional review: the hydrology of the Okavango Delta, Botswana—processes, data and modelling Christian Milzow & Lesego Kgotlhang & Peter Bauer-Gottwein & Philipp Meier & Wolfgang Kinzelbach Abstract The wetlands of the Okavango Delta accom- Introduction modate a multitude of ecosystems with a large diversity in fauna and flora. They not only provide the traditional The Okavango wetlands, commonly called the Okavango livelihood of the local communities but are also the basis Delta, are spread on top of an alluvial fan located in of a tourism industry that generates substantial revenue for northern Botswana, in the western branch of the East the whole of Botswana. For the global community, the African Rift Valley. Waters forming the Okavango River wetlands retain a tremendous pool of biodiversity. As the originate in the highlands of Angola, flow southwards, upstream states Angola and Namibia are developing, cross the Namibian Caprivi-Strip and eventually spread however, changes in the use of the water of the Okavango into the terminal wetlands on Botswanan territory cover- River and in the ecological status of the wetlands are to be ing the alluvial fan (Fig. 1). Whereas the climate in the expected. To predict these impacts, the hydrology of the headwater region is subtropical and humid with an annual Delta has to be understood. This article reviews scientific precipitation of up to 1,300 mm, it is semi-arid in Botswana work done for that purpose, focussing on the hydrological with precipitation amounting to only 450 mm/year in the modelling of surface water and groundwater. Research Delta area. High potential evapotranspiration rates cause providing input data to hydrological models is also over 95% of the wetland inflow and local precipitation to be presented. -
Altimetry, SAR and GRACE Applied for Modelling of an Ungauged Catchment
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Hydrol. Earth Syst. Sci. Discuss., 7, 9123–9154, 2010 Hydrology and www.hydrol-earth-syst-sci-discuss.net/7/9123/2010/ Earth System HESSD doi:10.5194/hessd-7-9123-2010 Sciences 7, 9123–9154, 2010 © Author(s) 2010. CC Attribution 3.0 License. Discussions Altimetry, SAR and This discussion paper is/has been under review for the journal Hydrology and Earth GRACE applied for System Sciences (HESS). Please refer to the corresponding final paper in HESS modelling of an if available. ungauged catchment Combining satellite radar altimetry, SAR C. Milzow et al. surface soil moisture and GRACE total Title Page storage changes for model calibration Abstract Introduction and validation in a large ungauged Conclusions References catchment Tables Figures 1 2 1 C. Milzow , P. E. Krogh , and P. Bauer-Gottwein J I 1 Department of Environmental Engineering, Technical University of Denmark, J I 2800 Kgs. Lyngby, Denmark 2National Space Institute, Technical University of Denmark, 2100 Copenhagen, Denmark Back Close Received: 12 November 2010 – Accepted: 20 November 2010 Full Screen / Esc – Published: 30 November 2010 Correspondence to: C. Milzow ([email protected]) Printer-friendly Version Published by Copernicus Publications on behalf of the European Geosciences Union. Interactive Discussion 9123 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract HESSD The availability of data is a major challenge for hydrological modelling in large -
Estimating Rainfall and Water Balance Over the Okavango River Baprovidedsin Byfor South Easthydrological Academic Libraries System (SEALS) Applications
View metadata, citation and similar papers at core.ac.uk brought to you by CORE Estimating rainfall and water balance over the Okavango River Baprovidedsin byfor South Easthydrological Academic Libraries System (SEALS) applications Julie Wilk, Dominic Kniveton, Lotta Andersson, Russell Layberry, Martin C. Todd, Denis Hughes, Susan Ringrose and Cornelis Vanderpost Department of Water and Environmental Studies, Linköping University, S-581 83 Linköping, Sweden Department of Physics Chemistry and Environmental Science, University of Sussex, Falmer, Brighton, UK Swedish Meteorological and Hydrological Institute, 601 76 Norrköping, Sweden University College of London, 26 Bedford Way, WC1H 0AP, London, UK Institute of Water Research, Rhodes University, Grahamstown, South Africa Harry Oppenheimer Okavango Research Centre, Private Bag 285, Maun, Botswana Abstract A historical database for use in rainfall-runoff modeling of the Okavango River Basin in Southwest Africa is presented. The work has relevance for similar data-sparse regions. The parameters of main concern are rainfall and catchment water balance, which are key variables for subsequent studies of the hydrological impacts of development and climate change. Rainfall estimates are based on a combination of in situ gauges and satellite sources. Rain gauge measurements are most extensive from 1955 to 1972, after which they are drastically reduced due to the Angolan civil war. The sensitivity of the rainfall fields to spatial interpolation techniques and the density of gauges were evaluated. Satellite based rainfall estimates for the basin are developed for the period from 1991 onwards, based on the Tropical Rainfall Measuring Mission (TRMM) and Special Sensor Microwave Imager (SSM/I) datasets. The consistency between the gauges and satellite estimates was considered. -
The Okavango; a River Supporting Its People, Environment and Economic Development
The Okavango; a river supporting its people, environment and economic development Article (Accepted Version) Kgathi, D L, Kniveton, D, Ringrose, S, Turton, A R, Vanderpost, C H M, Lundqvist, J and Seely, M (2006) The Okavango; a river supporting its people, environment and economic development. Journal of Hydrology, 331 (1-2). pp. 3-17. ISSN 0022-1694 This version is available from Sussex Research Online: http://sro.sussex.ac.uk/id/eprint/1690/ This document is made available in accordance with publisher policies and may differ from the published version or from the version of record. If you wish to cite this item you are advised to consult the publisher’s version. Please see the URL above for details on accessing the published version. Copyright and reuse: Sussex Research Online is a digital repository of the research output of the University. Copyright and all moral rights to the version of the paper presented here belong to the individual author(s) and/or other copyright owners. To the extent reasonable and practicable, the material made available in SRO has been checked for eligibility before being made available. Copies of full text items generally can be reproduced, displayed or performed and given to third parties in any format or medium for personal research or study, educational, or not-for-profit purposes without prior permission or charge, provided that the authors, title and full bibliographic details are credited, a hyperlink and/or URL is given for the original metadata page and the content is not changed in any way. http://sro.sussex.ac.uk Special Issue Journal of Hydrology The Hydrology of the Okavango Basin and Delta in a development perspective Guest editors: Dominic Kniveton, and Martin Todd Paper 1. -
Overview of the Cubango Okavango
Transboundary Cooperation for Protecting the Cubango- Okavango River Basin and Improving the Integrity of the Okavango Delta World Heritage Property Overview of the Cubango-Okavango River Basin in Angola: Challenges and Perspectives Maun, 3-4 June 2019 Botswana National Development Plan (2018-2022) The National Development Plan 6 Axis provides framework for the development of infrastructure, 25 Policies environmental sustainability and land and territorial planning. 83 Programs Cubango-Okavango River Basin Key Challenges To develop better conditions for the economic development of the region. To foster sustainable development considering technical, socio- economic and environmental aspects. To combat poverty and increase the opportunities of equitable socioeconomic benefits. Key Considerations 1. Inventory of the water needs and uses. 2. Assessment of the water balance between needs and availability. 3. Water quality. 4. Risk management and valorization of the water resources. Some of the Main Needs Water Institutional Monitoring Capacity Network Decision- Participatory making Management Supporting Systems Adequate Funding Master Plans for Cubango Zambezi and Basins Cubango/ Approved in 6 main Up to 2030 Okavango 2016 programs Final Draft 9 main Zambezi Up to 2035 2018 programs Cubango/Okavango Basin Master Plan Main Programs Rehabilitation of degraded areas. Maintaining the natural connectivity between rivers and river corridors. Implementing water monitoring network. Managing the fishery activity and water use. Biodiversity conservation. Capacity building and governance. Zambezi Basin Master Plan Main Programs Water supply for communities and economic activities. Sewage and water pollution control. Economic and social valorisation of water resources. Protection of ecosystems. Risk management. Economic sustainability of the water resources. Institutional and legal framework. -
Bloodlines: Mammals, Leeches, and Conservation in Southern Asia
Page 17 of 37 Systematics and Biodiversity 1 2 3 4 Bloodlines: mammals, leeches, and conservation in 5 6 7 southern Asia 8 9 10 1,2,3 4 3 11 MICHAEL TESSLER , SARAH R. WEISKOPF , LILY BERNIKER , REBECCA 12 13 HERSCH2, KYLE P. McCARTHY4, DOUGLAS W. YU5,6 & MARK E. SIDDALL1,2,3 14 15 16 17 1 18 Richard Gilder Graduate School, American Museum of Natural History, Central Park West at 19 20 79th Street, New York, NY 10024, USA 21 22 2Sackler Institute for Comparative Genomics, American Museum of Natural History, Central 23 24 25 Park West at 79th Street, New York, NY 10024, USA 26 3 27 Division of Invertebrate Zoology, American Museum of Natural History, Central Park West at 28 29 79th Street, New York, NY 10024, USA 30 31 4Department of Entomology and Wildlife Ecology, University of Delaware, 531 South College 32 33 34 Avenue, Newark, DE 19716, USA 35 36 5State Key Laboratory of Genetic Resources and Evolution, Kunming Institute of Zoology, 32 37 38 Jiaochang Dong Lu, Kunming, Yunnan 650223, China 39 40 6 41 School of Biological Sciences, University of East Anglia, Norwich Research Park, Norwich, 42 43 Norfolk NR4 7TJ UK 44 45 46 47 48 Running title: Mammals, leeches, and conservation 49 50 Correspondence to: Michael Tessler. E-mail: [email protected] 51 52 Southern Asia is a biodiversity hotspot both for terrestrial mammals and for leeches. Many 53 54 small-mammal groups are under-studied in this region, while other mammals are of known 55 56 57 58 59 60 URL: http://mc.manuscriptcentral.com/tsab Tessler et al. -
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J
Tropical Marine Invertebrates CAS BI 569 Phylum ANNELIDA by J. R. Finnerty Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “BILATERIA” (=TRIPLOBLASTICA) Bilateral symmetry (?) Mesoderm (triploblasty) Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA “COELOMATA” True coelom Coelomata gut cavity endoderm mesoderm coelom ectoderm [note: dorso-ventral inversion] Phylum ANNELIDA Porifera Ctenophora Cnidaria Deuterostomia Ecdysozoa Lophotrochozoa Chordata Arthropoda Annelida Hemichordata Onychophora Mollusca Echinodermata Nematoda Platyhelminthes Acoelomorpha Silicispongiae Calcispongia PROTOSTOMIA PROTOSTOMIA “first mouth” blastopore contributes to mouth ventral nerve cord The Blastopore ! Forms during gastrulation ectoderm blastocoel blastocoel endoderm gut blastoderm BLASTULA blastopore The Gut “internal, epithelium-lined cavity for the digestion and absorption of food sponges lack a gut simplest gut = blind sac (Cnidaria) blastopore gives rise to dual- function mouth/anus through-guts evolve later Protostome = blastopore contributes to the mouth Deuterostome = blastopore becomes the anus; mouth is a second opening Protostomy blastopore mouth anus Deuterostomy blastopore -
Leeches: a Review on Their Pathogenic and Beneficial Effects
ary Scien in ce er & t e T Aloto and Eticha, J Vet Sci Technol 2018, 9:1 V e f c h o Journal of Veterinary Science & n DOI: 10.4172/2157-7579.1000511 l o a l n o r g u y o J Technology ISSN: 2157-7579 Review Article Open Access Leeches: A Review on their Pathogenic and Beneficial Effects Desta Aloto1 and Eyob Eticha2* 1Veterinary Drug and Animal Feed Administration and Control Authority, South Region Branch Office, Hawassa, Ethiopia 2Asella Regional Veterinary Laboratory, PO Box 212, Ethiopia *Corresponding author: Eyob Eticha, Asella Regional Veterinary Laboratory, PO Box 212, Ethiopia, Tel: +251913178237; E-mail: [email protected] Rec date: December 23, 2017; Acc date: January 23, 2018; Pub date: January 24, 2018 Copyright: © 2018 Aloto D, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Abstract Leech is one of the external sanguivorous parasites contributing to the reduction in productivity of livestock in different part of the World. Leeches bite the skin of the host and allow copious flow of blood preventing clot by hirudin. The bite is not painful, but the wounds may bleed for a long time and the clinical signs can be seen following this blood loss. Types of leech vary depending on ways by which they feed. Leech is segmented and lacks as hard exoskeleton; in its place it has a thin, flexible cuticle. For the most part leeches are aquatic, but terrestrial species are also found. -
“Help, There Are Leeches in Our Lake!”
“Help, there are leeches in our lake!” by Andrea LaMoreaux, Vice President, NH LAKES “Help,” pleaded the caller, “Our lake is polluted—it is full of blood-sucking leeches!” As an aquatic biologist, this is one of the various reasons lake-goers call me during the summer, urging me to find someone or something to fix a problem that is ruining their enjoyment of one of New Hampshire’s approximately 1,000 lakes and ponds. “Don’t worry,” I explained, “Rest assured, by no means does the presence of leeches in your lake mean that your lake is polluted.” The caller on the other end of the phone was unconvinced, so I continued, “Leeches are natural organisms that can be found in most of New Hampshire’s lakes. While there are more than 650 species of leeches in North America, there Leeches are most commonly found in shallow areas are only a few species in New Hampshire known to take of lakes among plants, under rocks, sticks, logs, and blood from a person, and that is only if the right attached to decaying leaves. opportunity arises.” At this point, I emailed the caller some information about where leeches are found, what to do if he got bit by a leech, and how to avoid leaches altogether. I never got a return call back, so I guessed his fears were quelled. In case you aren’t convinced that leeches aren’t a problem, or if you are just curious… What are leeches and where are they found? Leeches are scientifically categorized as annelids (segmented worms) and they are closely related to earthworms.